A view from the grassy meadow west of Seafield House (1885) - Westward Ho!.
Beach deposits of sandstone cobbles in a sandy matrix lying on an ancient wave cut platform , left high and dry when sea levels fell 125,000 years ago.
Covered with head from the period 10,000 - 100,000 years ago when periglacial conditions - freeze / thaw cycles caused the rock to fragment into a layer of angular stones and small debris.

Raised Beach

A view from the grassy meadow west of Seafield House (1885) - Westward Ho!.
Beach deposits of sandstone cobbles in a sandy matrix lying on an ancient wave cut platform , left high and dry when sea levels fell 125,000 years ago.
Covered with head from the period 10,000 - 100,000 years ago when periglacial conditions - freeze / thaw cycles caused the rock to fragment into a layer of angular stones and small debris.

Raised Beach

A view from the grassy meadow west of Seafield House (1885) - Westward Ho!.
Beach deposits of sandstone cobbles in a sandy matrix lying on an ancient wave cut platform , left high and dry when sea levels fell 125,000 years ago.
Covered with head from the period 10,000 - 100,000 years ago when periglacial conditions - freeze / thaw cycles caused the rock to fragment into a layer of angular stones and small debris.

Raised Beach

A view from the grassy meadow west of Seafield House (1885) - Westward Ho!.
Beach deposits of sandstone cobbles in a sandy matrix lying on an ancient wave cut platform , left high and dry when sea levels fell 125,000 years ago.
Covered with head from the period 10,000 - 100,000 years ago when periglacial conditions - freeze / thaw cycles caused the rock to fragment into a layer of angular stones and small debris.